Resolving the scale dependency in laboratory and field weathering rates
Results from tracer studies in hydraulically-unsaturated column reactors containing mine rockdemonstrate that significant mass of pore water is relatively immobile. This water mass is retained within stagnant zones that do not contribute to advective transport of solutes in reactor effluent. Solutes...
| Main Authors: | , , |
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| Format: | Conference Paper |
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Taylor and Francis Group
2004
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/3961 |